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Sumo Has Landed in Regional NSW! May 2021
Sumo has landed in Regional NSW! May 2021 Sumo has expanded into over a thousand new suburbs! Postcode Suburb Distributor 2580 BANNABY Essential 2580 BANNISTER Essential 2580 BAW BAW Essential 2580 BOXERS CREEK Essential 2580 BRISBANE GROVE Essential 2580 BUNGONIA Essential 2580 CARRICK Essential 2580 CHATSBURY Essential 2580 CURRAWANG Essential 2580 CURRAWEELA Essential 2580 GOLSPIE Essential 2580 GOULBURN Essential 2580 GREENWICH PARK Essential 2580 GUNDARY Essential 2580 JERRONG Essential 2580 KINGSDALE Essential 2580 LAKE BATHURST Essential 2580 LOWER BORO Essential 2580 MAYFIELD Essential 2580 MIDDLE ARM Essential 2580 MOUNT FAIRY Essential 2580 MOUNT WERONG Essential 2580 MUMMEL Essential 2580 MYRTLEVILLE Essential 2580 OALLEN Essential 2580 PALING YARDS Essential 2580 PARKESBOURNE Essential 2580 POMEROY Essential ©2021 ACN Inc. All rights reserved ACN Pacific Pty Ltd ABN 85 108 535 708 www.acn.com PF-1271 13.05.2021 Page 1 of 31 Sumo has landed in Regional NSW! May 2021 2580 QUIALIGO Essential 2580 RICHLANDS Essential 2580 ROSLYN Essential 2580 RUN-O-WATERS Essential 2580 STONEQUARRY Essential 2580 TARAGO Essential 2580 TARALGA Essential 2580 TARLO Essential 2580 TIRRANNAVILLE Essential 2580 TOWRANG Essential 2580 WAYO Essential 2580 WIARBOROUGH Essential 2580 WINDELLAMA Essential 2580 WOLLOGORANG Essential 2580 WOMBEYAN CAVES Essential 2580 WOODHOUSELEE Essential 2580 YALBRAITH Essential 2580 YARRA Essential 2581 BELLMOUNT FOREST Essential 2581 BEVENDALE Essential 2581 BIALA Essential 2581 BLAKNEY CREEK Essential 2581 BREADALBANE Essential 2581 BROADWAY Essential 2581 COLLECTOR Essential 2581 CULLERIN Essential 2581 DALTON Essential 2581 GUNNING Essential 2581 GURRUNDAH Essential 2581 LADE VALE Essential 2581 LAKE GEORGE Essential 2581 LERIDA Essential 2581 MERRILL Essential 2581 OOLONG Essential ©2021 ACN Inc. -
Management Plan Conservation Reserve
Jenolan Karst Conservation Reserve Conservation Management Plan Volume 1 : Report August 2009 Conservation Management Plan property address month & year only Conservation Management Plan Volume 1of 2 - Report Prepared for Jenolan Caves Reserve Trust and the NSW Department of Environment and Climate Change August 2009 TABLE OF CONTENTS Executive Summary ..................................................................................................................................i 1 Introduction ....................................................................................................................................1 1.1 The Jenolan Karst Conservation Reserve .......................................................................................1 1.2 Scope of the Report .........................................................................................................................1 1.3 Aims of the Report............................................................................................................................1 1.4 Structure of the Report.....................................................................................................................2 1.5 Site Ownership.................................................................................................................................2 1.6 Site Location.....................................................................................................................................2 1.7 Site Visits..........................................................................................................................................2 -
Gauging Station Index
Site Details Flow/Volume Height/Elevation NSW River Basins: Gauging Station Details Other No. of Area Data Data Site ID Sitename Cat Commence Ceased Status Owner Lat Long Datum Start Date End Date Start Date End Date Data Gaugings (km2) (Years) (Years) 1102001 Homestead Creek at Fowlers Gap C 7/08/1972 31/05/2003 Closed DWR 19.9 -31.0848 141.6974 GDA94 07/08/1972 16/12/1995 23.4 01/01/1972 01/01/1996 24 Rn 1102002 Frieslich Creek at Frieslich Dam C 21/10/1976 31/05/2003 Closed DWR 8 -31.0660 141.6690 GDA94 19/03/1977 31/05/2003 26.2 01/01/1977 01/01/2004 27 Rn 1102003 Fowlers Creek at Fowlers Gap C 13/05/1980 31/05/2003 Closed DWR 384 -31.0856 141.7131 GDA94 28/02/1992 07/12/1992 0.8 01/05/1980 01/01/1993 12.7 Basin 201: Tweed River Basin 201001 Oxley River at Eungella A 21/05/1947 Open DWR 213 -28.3537 153.2931 GDA94 03/03/1957 08/11/2010 53.7 30/12/1899 08/11/2010 110.9 Rn 388 201002 Rous River at Boat Harbour No.1 C 27/05/1947 31/07/1957 Closed DWR 124 -28.3151 153.3511 GDA94 01/05/1947 01/04/1957 9.9 48 201003 Tweed River at Braeside C 20/08/1951 31/12/1968 Closed DWR 298 -28.3960 153.3369 GDA94 01/08/1951 01/01/1969 17.4 126 201004 Tweed River at Kunghur C 14/05/1954 2/06/1982 Closed DWR 49 -28.4702 153.2547 GDA94 01/08/1954 01/07/1982 27.9 196 201005 Rous River at Boat Harbour No.3 A 3/04/1957 Open DWR 111 -28.3096 153.3360 GDA94 03/04/1957 08/11/2010 53.6 01/01/1957 01/01/2010 53 261 201006 Oxley River at Tyalgum C 5/05/1969 12/08/1982 Closed DWR 153 -28.3526 153.2245 GDA94 01/06/1969 01/09/1982 13.3 108 201007 Hopping Dick Creek -
Introduction to Virginia's Karst
Introduction to Virginia’s Karst A presentation of The Virginia Department of Conservation and Recreation’s Karst Program & Project Underground Karst - A landscape developed in limestone, dolomite, marble, or other soluble rocks and characterized by subsurface drainage systems, sinking or losing streams, sinkholes, springs, and caves. Cross-section diagram by David Culver, American University. Karst topography covers much of the Valley and Ridge Province in the western third of the state. Aerial photo of karst landscape in Russell County. Smaller karst areas also occur in the Cumberland Plateau, Piedmont, and Coastal Plain provinces. At least 29 counties support karst terrane in western Virginia. In western Virginia, karst occurs along slopes and in valleys between mountain ridges. There are few surface streams in these limestone valleys as runoff from mountain slopes disappears into the subsurface upon contact with the karst bedrock. Water flows underground, emerging at springs on the valley floor. Thin soils over fractured, cavernous limestone allow precipitation to enter the subsurface directly and rapidly, with a minimal amount of natural filtration. The purer the limestone, the less soil develops on the bedrock, leaving bare pinnacles exposed at the ground surface. Rock pinnacles may also occur where land use practices result in massive soil loss. Precipitation mixing with carbon dioxide becomes acidic as it passes through soil. Through geologic time slightly acidic water dissolves and enlarges the bedrock fractures, forming caves and other voids in the bedrock. Water follows the path of least resistance, so it moves through voids in rock layers, fractures, and boundaries between soluble and insoluble bedrock. -
Parramatta's Archaeological Landscape
Parramatta’s archaeological landscape Mary Casey Settlement at Parramatta, the third British settlement in Australia after Sydney Cove and Norfolk Island, began with the remaking of the landscape from an Aboriginal place, to a military redoubt and agricultural settlement, and then a township. There has been limited analysis of the development of Parramatta’s landscape from an archaeological perspective and while there have been numerous excavations there has been little exploration of these sites within the context of this evolving landscape. This analysis is important as the beginnings and changes to Parramatta are complex. The layering of the archaeology presents a confusion of possible interpretations which need a firmer historical and landscape framework through which to interpret the findings of individual archaeological sites. It involves a review of the whole range of maps, plans and images, some previously unpublished and unanalysed, within the context of the remaking of Parramatta and its archaeological landscape. The maps and images are explored through the lense of government administration and its intentions and the need to grow crops successfully to sustain the purposes of British Imperialism in the Colony of New South Wales, with its associated needs for successful agriculture, convict accommodation and the eventual development of a free settlement occupied by emancipated convicts and settlers. Parramatta’s river terraces were covered by woodlands dominated by eucalypts, in particular grey box (Eucalyptus moluccana) and forest -
California's Coastal Sea Caves, NSS News, October 1998
California’s Coastal Sea Caves by Dave Bunnell Large chamber in Cave-in-Rock Cave, San Luis Obispo County elmets, lights, wetsuits, fins, face California, with its more accessible caves, are undoubtedly caves in Humboldt and Del masks and snorkels, vertical gear, has yielded as many again to the surveyor’s Norte counties, no survey work has been H and sea kayaks were not what I was tape and doubtless many more remain, undertaken there. I’ll begin with the southern used to packing for a cave trip until I especially in the remote northern counties. counties, for that was the original focus of moved to California. But after a couple of Much has been published over the years in sea cave survey. years of caving here, I realized that there were grotto and regional publications, but this is large numbers of caves here that had been the first time I’ve written an overall summary SAN DIEGO COUNTY largely ignored. After all, what caver wants of the Survey’s work on coastal caves. Perhaps the most famous of the sea caves to spend his weekends at the beach? on the California coast are the “seven caves” Systematic exploration and survey of GENERALITIES at La Jolla, formed in a 200’ high cliff of California’s many sea caves really began While not as large on average as the Cretaceous-age sandstone. A perennial when Carol Vesely and I chartered the island caves, the coastal caves are found in tourist favorite, La Jolla Cove and its cavey Southern California Sea Cave Survey in numerous host rocks that lend diverse cliffs are featured on dozens of old postcards. -
Bathurst Region Destination Planner
2020 DESTINATION PLANNER BATHURSTREGION.COM.AU Bathurst is a city of contrasts in one of the most fascinating and diverse regions of NSW. Heritage listed buildings and world class museums and galleries are only a part of the rich history on offer, whilst spectacular natural wonders co-exist with a modern cultural landscape and the lively villages that surround the city. KING’S PARADE If there is one thing you can expect from lap of the circuit and visiting the National Bathurst it’s the unexpected. A city of Motor Racing Museum. BATHURST COURTHOUSE surprises, a historical town brought Mixing the new and exciting with its right up to the moment by the people heritage is what Bathurst is all about – who live and work here. Bathurst is a there truly is something for everyone here. city of contrasts, from the heritage listed buildings to quirky bars and restaurants, modern accommodation and a host of arts, Bathurst Visitor Information Centre crafts and music events in the surrounding The Bathurst Visitor Information Centre areas guaranteed to delight. One moment (known affectionately as BVIC to the locals) you can be exploring the heritage Town is the proud heart of the Bathurst region. Square guided by local Grant Denyer on Call in and visit the friendly team. We love the Bathurst Step Beyond App, the next what we do and no one knows the best of sitting in a cosy cafe sipping a latte or in a the region like us. Begin your adventures new restaurant trying an innovative dish. and chat with a local expert at the Bathurst Or walking through the impressive T.Arts Visitor Information Centre. -
Deua National Park
AUSTRALIA THE AUSTRALIAN c A, ER SPELEOLOGICAL QUARTERLY ~ II No.IIO 1986 II Registered by Australia Post Publication Number NBQ 5116 HEHBKR SOCIETIES & ASSOCIATED ORGANISATIONS COUNCIL HEHBKRS ACT: Canberra Speleological Society 18 Arabana St Aranda ACT 2614 Capital Territory Caving Group PO Box 638 Woden ACT 2606 National University Caving Club c/-Sports Union Australian National university ACT 2600 NSW: Baptist Caving Association 90 Parkes St Helensburg NSW 2508 Blue Mountains Speleological Club PO Box37 Glenbrook NSW 2773 Endeavour Caving & Recreational Club PO Box 63 Miranda NSW 2228 Highland Caving Group PO Box 154 Liverpool NSW 2170 Hills Speoleology Club PO Box 198 Baulkharn Hills NSW 2153 Illawarra Speleological Society PO Box 94 Unanderra NSW 2526 Kempsey Speleological Society 27 River St Kempsey NSW 2440 Macquarie University Caving Group c/-Sports Association Macquarie Uni Nth Ryde NSW 211 3 Metropolitan Speleological Society PO Box 2376 Nth Parramatta NSW 2151 Newcastle And Hunter Valley Speleological Society PO Box 15 Broadrneadow NSW 2292 NSW Institute Of Technology Speleological Society c/-The Union PO Box 123 Broadway NSW 2007 Orange Speleological Society PO Box 752 Orange NSW 2800 RAN Caving Association c/- 30 Douglas Ave Nth Epping NSW 2121 Sydney University Speleological Society Box 35 The Union Sydney University NSW 2006 University Of NSW Speleological Society Box 17 The Union UNSW Kensington NSW 2033 QUEENSLAND: Central Queensland Speleological Society PO Box 538 Rockhampton Qld 4700 University Of Queensland Speleological -
Water Sharing Plan for Lachlan Unregulated and Alluvial Water Sources 2012
LOCALITY MAP Key to Extraction Management Units LACHLAN UNREGULATED EXTRACTION MANAGEMENT UNIT YATHONG RD Til Creek Eremaran Creek Burthong Creek Keginni Creek Thule Creek MERRI RD NYMAGEE CONDOBOLIN RD COBB HWY Marobee Creek COBAR-IVANHOE RD MOUNT HOPE AREA WATER SOURCE Yarran Creek Carlisle Creek ! Mount Hope Murda Creek Ivanhoe Coombie Creek Cogie Creek Conoble ! Gillenbine Creek Piccaninny Creek Lake ! Trundle GILGUNNIA RD GUNNINGBLAND AND YARRABANDAI WATER SOURCE NEWELL HWY Waterloo Lake Goobang Creek Purcells ROTO RD Back Creek Lake PARKES-CONDOBOLIN RD Manildra Creek Conoble Creek Gumble Creek Waverley Creek Blowclear Creek Beargamil Creek BALRANALD RD MID LACHLAN UNREGULATED WATER SOURCE ! Gunningbland Creek Whipstick Yarrabandai Creek Billabong Creek CONDOBOLIN RD Lake Wallaroi Creek Condobolin Parkes ORANGE RD Mitchells Creek Ridgey Creek ! Wallamundry Creek Manildra Willandra Creek Coates Creek ! Lachlan River MITCHELL HWY ! Willandra Creek Lachlan River GOOBANG AND BILLABONG CREEKS WATER SOURCE Boree Creek Barneys Crooked Creek Reedy Creek Lake Willandra Yangellawah Creek Banar Island Creek Lake Spring Creek Cudal CLARE MOSSGIEL RD Goobang Creek HILLSTON MOSSGIEL RD Bogan MANDAGERY CREEK WATER SOURCE dillon ! Bourimbla Creek Lake ! Paling Yard Creek Lake Swamp Cargelligo Warree Creek see INSET Cargelligo THE GIPPS WAY Waterhole Creek Mandagery Creek Alma Moolbong Creek Tullibigeal Forbes Lake Christmas Creek Mountain Creek ! Once Awhile Creek WYALONG RD THE ESCORT WAY Mogong Creek CANOWINDRA RD ! ! Eugowra Cowriga Creek BOGANDILLON -
Annual Report 2001-2002 (PDF
2001 2002 Annual report NSW national Parks & Wildlife service Published by NSW National Parks and Wildlife Service PO Box 1967, Hurstville 2220 Copyright © National Parks and Wildlife Service 2002 ISSN 0158-0965 Coordinator: Christine Sultana Editor: Catherine Munro Design and layout: Harley & Jones design Printed by: Agency Printing Front cover photos (from top left): Sturt National Park (G Robertson/NPWS); Bouddi National Park (J Winter/NPWS); Banksias, Gibraltar Range National Park Copies of this report are available from the National Parks Centre, (P Green/NPWS); Launch of Backyard Buddies program (NPWS); Pacific black duck 102 George St, The Rocks, Sydney, phone 1300 361 967; or (P Green); Beyers Cottage, Hill End Historic Site (G Ashley/NPWS). NPWS Mail Order, PO Box 1967, Hurstville 2220, phone: 9585 6533. Back cover photos (from left): Python tree, Gossia bidwillii (P Green); Repatriation of Aboriginal remains, La Perouse (C Bento/Australian Museum); This report can also be downloaded from the NPWS website: Rainforest, Nightcap National Park (P Green/NPWS); Northern banjo frog (J Little). www.npws.nsw.gov.au Inside front cover: Sturt National Park (G Robertson/NPWS). Annual report 2001-2002 NPWS mission G Robertson/NPWS NSW national Parks & Wildlife service 2 Contents Director-General’s foreword 6 3Conservation management 43 Working with Aboriginal communities 44 Overview Joint management of national parks 44 Mission statement 8 Aboriginal heritage 46 Role and functions 8 Outside the reserve system 47 Customers, partners and stakeholders -
Museum of Natural History & Science Interpretation Guide for the Cavern
Museum of Natural History & Science Interpretation Guide for The Cavern A cave is a naturally occurring hole in the ground large enough to be explored by humans. Caves can be found on every continent in the world. Caves, along with the objects found within them, are extremely fragile and take millions of years to form. They are home to unique organisms—many of which are still unknown to science; they are archaeological sites that preserve our cultural heritage; and geologic laboratories that demonstrate how water can both dissolve and deposit rock. Caves are a vital and non-renewable resource that must be conserved and protected. The Cavern is a recreation of a Kentucky limestone dissolution cave. It is the largest artificial cave in the United States—and some say the world—containing 535 feet of passage in an area 44 feet wide, 24 feet high and 64 feet long. Parts of the cave were modeled after two caves in Kentucky: Teamers Cave in Rockcastle County and Dyches Bridge Cave in Pulaski County. By modeling our cavern after these two caves, our dissolution cave has a realistic appearance. A dissolution cave is by far the most common type of cave. They can be found throughout the world if the right conditions present themselves. The formation of a dissolution cave requires four basic elements: rock, water, carbon dioxide and time. • Rock, especially carbonate rocks, such as limestone, is the first ingredient. These types of rocks were formed hundreds of millions of years ago. It is in the seas surrounding the continents that limestone is formed. -
Beaches Unit (4.5 Pts) Section
T. James Noyes, El Camino College Beaches Unit (Topic 6A) – page 1 Name: Beaches Unit (4.5 pts) Section: Beaches and Shorelines are always changing Waves are slowly and inexorably altering the shoreline, breaking down material in some places and carrying it to other places. Each wave has a small effect, but waves keep coming minute after minute, day after day, year after year. Significant changes in the shoreline (tens of feet) can occur within a human lifetime. For example, old maps of Encinitas (located along the coastal cliffs by Interstate 5 on the way down to San Diego) show that it has lost about a city block of land to the sea in the last century. In some places along the coast of Alaska, the shoreline has eroded 900 meters in 50 years, an average of about 18 meters (60 feet) per year! Beach Sediments Beach sediments are composed of whatever sediments are available locally: sand, cobbles, gravel, coral fragments, shell fragments, and so on. (In fact, tiny plastic sediments are making up a larger and larger component of our beaches.) Beach sediments are characterized by (1) the kind of material that they are made out of, (2) their size, (3) their shape, and (4) their sorting. (Well sorted sediments all have about the same size and shape, while poorly sorted sediments are a jumbled mix of sediments with many different sizes and shapes. Lithogenous sediments (“rock sediments”) are produced from the weathering of the rock of the land. Rocks are broken down into pieces (sediments) by the physical impact of water, wind, and other rocks; by chemicals dissolved in water; and repeated heating and cooling.